% This file contains a station summary listing for a temperature % station in the Berkeley Earth database. This station is identified as: % % Berkeley ID#: 39799 % Primary Name: WOONSOCKET % Record Type: TAVG % Country: United States % State: SD % Latitude: 44.05000 +/- 0.00005 % Longitude: -98.26670 +/- 0.00005 % Elevation (m): 399.90 +/- 0.05 % # of Months: 12 % % Alternate Names: WOONSOCKET 2 W % WOONSOCKET 5 S % WOONSOCKET 5 SW % % IDs: coop - 399457 % ghcnd - USC00399457 % ncdc - 20017738 % % Sources: US Cooperative Summary of the Day % Global Historical Climatology Network - Daily % US Cooperative Summary of the Month % Multi-network Metadata System % % Site Hash: ecfd964bff8479a5e21aefec030725db % Raw Data Hash: b111bbce0e5b71bfdf40ab538d62772b % Adj Data Hash: a616509bd41fda857dac486030ede310 % % The data for this station is presented below in several columns and in % several forms. The temperature values are reported as "raw", % "adjusted", and "regional expectation". % % The "raw" values reflect the observations as originally ingested by % the Berkeley Earth system from one or more originating archive(s). % These "raw" values may reflect the merger of more than one temperature % time series if multiple archives reported values for this location. % Alongside the raw data we have also provided a flag indicating which % values failed initial quality control checks. A further column % dates at which the raw data may be subject to continuity "breaks" % due to documented station moves (denoted "1"), prolonged measurement % gaps (denoted "2"), documented time of observation changes (denoted "3") % and other empirically determined inhomogeneities (denoted "4"). % % In many cases, raw temperature data contains a number of artifacts, % caused by issues such as typographical errors, instrumentation changes, % station moves, and urban or agricultural development near the station. % The Berkeley Earth analysis process attempts to identify and estimate % the impact of various kinds of data quality problems by comparing each % time series to neighboring series. At the end of the analysis process, % the "adjusted" data is created as an estimate of what the weather at % this location might have looked like after removing apparent biases. % This "adjusted" data will generally to be free from quality control % issues and be regionally homogeneous. Some users may find this % "adjusted" data that attempts to remove apparent biases more % suitable for their needs, while other users may prefer to work % with raw values. % % Lastly, we have provided a "regional expectation" time series, based % on the Berkeley Earth expected temperatures in the neighborhood of the % station. This incorporates information from as many weather stations as % are available for the local region surrounding this location. Note % that the regional expectation may be a systematically a bit warmer or % colder than the weather stations by a few degrees due to differences % in mean elevation and other local characteristics. % % For each temperature time series, we have also included an "anomaly" % time series that removes both the seasonality and the long-term mean. % These anomalies may provide an easier way of seeing changes through % time. % % Reported temperatures are in Celsius and reflect monthly averages. As % these files are intended to be summaries for convenience, additional % information, including more detailed flagging and metadata, may be % available in our whole data set files. % % The Berkeley Earth analysis was run on 15-Nov-2013 19:55:48 % % Raw Data QC Continuity Adjusted Data Regional Expectation % Year, Month, Temperature, Anomaly, Failed, Breaks, Temperature, Anomaly, Temperature, Anomaly 1939 4 NaN NaN NaN NaN NaN NaN 7.543 -0.093 1939 5 NaN NaN NaN NaN NaN NaN 18.081 3.674 1939 6 NaN NaN NaN NaN NaN NaN 19.638 -0.253 1939 7 NaN NaN NaN NaN NaN NaN 24.986 1.721 1939 8 NaN NaN NaN NaN NaN NaN 22.449 0.173 1939 9 NaN NaN NaN NaN NaN NaN 18.614 2.178 1939 10 NaN NaN NaN NaN NaN NaN 9.893 0.208 1939 11 NaN NaN NaN NaN NaN NaN 3.331 2.973 1939 12 NaN NaN NaN NaN NaN NaN -1.301 5.753 1940 1 NaN NaN NaN NaN NaN NaN -16.553 -5.385 1940 2 NaN NaN NaN NaN NaN NaN -7.114 0.094 1940 3 NaN NaN NaN NaN NaN NaN -3.418 -2.176 1940 4 7.838 -1.483 1 0 NaN NaN 6.650 -0.987 1940 5 NaN NaN NaN NaN NaN NaN 13.843 -0.564 1940 6 22.185 0.610 0 0 22.185 0.610 19.910 0.019 1940 7 26.406 1.458 0 0 26.406 1.458 25.558 2.294 1940 8 21.948 -2.011 0 0 21.948 -2.011 21.522 -0.754 1940 9 20.897 2.777 0 0 20.897 2.777 19.203 2.767 1940 10 NaN NaN NaN NaN NaN NaN 13.833 4.148 1940 11 NaN NaN NaN NaN NaN NaN -2.487 -2.845 1940 12 -1.885 3.485 0 0 -1.885 3.485 -4.347 2.707 1941 1 -5.895 3.589 0 0 -5.895 3.589 -9.758 1.410 1941 2 NaN NaN NaN NaN NaN NaN -7.896 -0.688 1941 3 NaN NaN NaN NaN NaN NaN -1.988 -0.746 1941 4 NaN NaN NaN NaN NaN NaN 9.734 2.098 1941 5 18.913 2.822 0 0 18.913 2.822 17.197 2.790 1941 6 21.563 -0.012 0 0 21.563 -0.012 19.742 -0.150 1941 7 25.406 0.458 0 0 25.406 0.458 24.437 1.173 1941 8 24.616 0.657 0 0 24.616 0.657 23.752 1.477 1941 9 18.415 0.295 0 0 18.415 0.295 16.833 0.397 1941 10 NaN NaN NaN NaN NaN NaN 10.325 0.641 1941 11 NaN NaN NaN NaN NaN NaN 1.910 1.553 1941 12 NaN NaN NaN NaN NaN NaN -2.592 4.463 1942 1 NaN NaN NaN NaN NaN NaN -6.678 4.490 1942 2 NaN NaN NaN NaN NaN NaN -6.281 0.928 1942 3 NaN NaN NaN NaN NaN NaN -0.065 1.177 1942 4 NaN NaN NaN NaN NaN NaN 10.603 2.966 1942 5 NaN NaN NaN NaN NaN NaN 11.890 -2.518 1942 6 NaN NaN NaN NaN NaN NaN 18.430 -1.462 1942 7 NaN NaN NaN NaN NaN NaN 22.021 -1.244 1942 8 NaN NaN NaN NaN NaN NaN 21.854 -0.421 1942 9 NaN NaN NaN NaN NaN NaN 13.256 -3.180